Precambrian volcanic rocks polished and grooved
- WOK 3-108
- Item
- 1954
Parte de W.O. Kupsch fonds
Precambrian volcanic rocks polished and grooved by glacier action. Flin Flon, Manitoba.
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Precambrian volcanic rocks polished and grooved
Parte de W.O. Kupsch fonds
Precambrian volcanic rocks polished and grooved by glacier action. Flin Flon, Manitoba.
Glacial valley Beartooth Mountains, Montana
Parte de W.O. Kupsch fonds
Glacial valley Beartooth Mountains, Montana.
Grooved and polished quartzite
Parte de W.O. Kupsch fonds
Grooved and polished quartzite; Great Cloche Island, Ontario.
Index map - Moose Mountain area
Parte de W.O. Kupsch fonds
Index map - Moose Mountain area.
Index to maps covering Moose Mountain area
Parte de W.O. Kupsch fonds
Index to maps covering Moose Mountain area.
Glacial history Moose Mountain area - phase No. 3
Parte de W.O. Kupsch fonds
Glacial history Moose Mountain area - phase No. 3.
Glacial history Moose Mountain area - phase No. 4
Parte de W.O. Kupsch fonds
Glacial history Moose Mountain area - phase No. 4.
Lake rampart, Sucker Lake, north of Shellbrook, Sask.
Parte de W.O. Kupsch fonds
Lake rampart, Sucker Lake, north of Shellbrook, Sask.
Old spruce tree on lake rampart
Parte de W.O. Kupsch fonds
Old spruce tree on lake rampart.
Earth flow near Fort Qu'Appelle, spring 1956
Parte de W.O. Kupsch fonds
Earth flow near Fort Qu'Appelle, spring 1956.
Alluvial fan from tributary into Qu'Appelle Valley - Katepwa, Saskatchewan
Parte de W.O. Kupsch fonds
Alluvial fan from tributary into Qu'Appelle Valley near Katepwa, Saskatchewan.
Sem título
Parte de W.O. Kupsch fonds
Flutings near Katepwa, Sask.
Straight ice marginal channel - west of Wawota, Sask.
Parte de W.O. Kupsch fonds
Straight ice marginal channel. Along highway 16, about 4 miles west of Wawota, Sask.
Deformation in Ravenscrag sands - near Hallbrite, Sask.
Parte de W.O. Kupsch fonds
Deformation in Ravenscrag sands probably due to ice push. Near Hallbrite, Sask.
Drag folds in Ravenscrag sand - near Hallbrite, Sask.
Parte de W.O. Kupsch fonds
Drag folds in Ravenscrag sand probably due to ice push. Near Hallbrite, Sask.